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    东营凹陷细粒混积岩发育环境及其岩相组合:以沙四上亚段泥页岩细粒沉积为例

    刘惠民 王勇 杨永红 张顺

    刘惠民, 王勇, 杨永红, 张顺, 2020. 东营凹陷细粒混积岩发育环境及其岩相组合:以沙四上亚段泥页岩细粒沉积为例. 地球科学, 45(10): 3543-3555. doi: 10.3799/dqkx.2020.156
    引用本文: 刘惠民, 王勇, 杨永红, 张顺, 2020. 东营凹陷细粒混积岩发育环境及其岩相组合:以沙四上亚段泥页岩细粒沉积为例. 地球科学, 45(10): 3543-3555. doi: 10.3799/dqkx.2020.156
    Liu Huimin, Wang Yong, Yang Yonghong, Zhang Shun, 2020. Sedimentary Environment and Lithofacies of Fine-Grained Hybrid Sedimentary in Dongying Sag: A Case of Fine-Grained Sedimentary System of the Es4. Earth Science, 45(10): 3543-3555. doi: 10.3799/dqkx.2020.156
    Citation: Liu Huimin, Wang Yong, Yang Yonghong, Zhang Shun, 2020. Sedimentary Environment and Lithofacies of Fine-Grained Hybrid Sedimentary in Dongying Sag: A Case of Fine-Grained Sedimentary System of the Es4. Earth Science, 45(10): 3543-3555. doi: 10.3799/dqkx.2020.156

    东营凹陷细粒混积岩发育环境及其岩相组合:以沙四上亚段泥页岩细粒沉积为例

    doi: 10.3799/dqkx.2020.156
    基金项目: 

    国家重点基础研究发展规划“973”项目 2014CB239100

    国家重点专项项目 2017ZX05049

    详细信息
      作者简介:

      刘惠民(1969-), 男, 教授级高级工程师, 博士, 从事胜利油田分公司油气勘探研究与管理工作.ORCID:0000-0003-3022-3873.E-mail:hmliu@vip.163.com

    • 中图分类号: P618.13

    Sedimentary Environment and Lithofacies of Fine-Grained Hybrid Sedimentary in Dongying Sag: A Case of Fine-Grained Sedimentary System of the Es4

    • 摘要: 为了进行陆相断陷湖盆泥页岩细粒混积岩有利岩相预测,以指导页岩油气有利目标优选,综合运用岩心、薄片、全岩衍射、元素、古生物等资料,系统进行了东营凹陷沙四上亚段泥页岩细粒混积岩沉积环境恢复、岩相精细表征,揭示了沉积环境对岩相及其组合、分布的控制作用.研究表明,东营凹陷沙四上亚段泥页岩细粒混积岩沉积期整体上表现为气候由半湿润向湿润转化,自下而上显示碎屑物源输入量在增加、水体水深加大、盐度降低、还原性减弱的过程;有序复杂多变的沉积环境一定程度上控制了泥页岩细粒混积岩沉积组构复杂性,进而控制了细粒混积岩相的多样性、组合和分布规律性.建立基于“岩石组分、沉积构造、灰质结构和有机质丰度”四端元划分方案,将东营凹陷沙四上亚段泥页岩细粒混积岩划分为20类,实现了复杂细粒混积岩岩相划分;半湿润少物源条件下,浅湖强还原盐水环境主要发育膏盐、含有机质层状膏质泥岩和含有机质层状泥质灰(云)岩相组合,半深湖强还原咸水环境主要发育富有机质纹层状微晶泥质灰岩和富有机质纹层状灰质泥岩频繁互层岩相组合,半深湖强还原半咸水环境主要发育富有机质水平泥晶纹层泥质灰岩和富有机质纹层灰质泥岩频繁互层岩相组合,深湖还原半咸水环境主要发育富有机质层状泥质灰岩夹富有机质层状灰质泥岩相组合;湿润多物源条件下,深湖强还原半咸水环境主要发育富有机质层状泥质灰岩和富有机质层状灰质泥岩频繁互层岩相组合,深湖还原半咸水环境主要发育富有机质层状灰质泥岩夹富有机质层状泥质灰岩相组合.

       

    • 图  1  沉积环境微观照片

      a.膏质泥岩,石膏燕尾双晶,Ny1井,3 492.08 m;b.含有机质层状膏质泥岩,盐晶粒,Ny1井,3 492.50 m; c.含有机质块状粉砂质泥岩,贝壳,Ny1井,3 467.08 m;d.超微化石富集层,Ny1井,3 424.29 m

      Fig.  1.  Photos of sedimentary environment

      图  2  孢粉与气候干湿指数关系图(Hk1井)

      Fig.  2.  Relationship between palynology and climatic dry and wet index (well Hk1)

      图  3  东营凹陷沙四上亚段沉积环境与岩相组合

      Fig.  3.  Sedimentary environment and lithofacies association of the upper Es4, submember in Dongying depression

      图  4  主要岩相类型及特征

      Fig.  4.  The types and characteristics of main lithofacies

      图  5  泥页岩细粒沉积作用

      Fig.  5.  The process of fine-grained deposition of fine-grained mud shale

      图  6  东营凹陷沙四上2层组沉积期古水深、古盐度、有机质含量等值线及沉积构造分布

      Fig.  6.  Paleodepth, paleosalinity, organic matter content contour map and sedimentary structure distribution map of Shasi upper 2 Formation in Dongying depression

      表  1  东营凹陷细粒混积岩岩相类型划分方案

      Table  1.   Classification scheme of fine-grained mixed rock facies in Dongying depression

      岩相类型 岩石组分 碳酸盐岩晶粒大小 沉积构造(纹层厚度) 有机质丰度(TOC)
      富有机质纹层状泥岩 Vsh≥75% < 4 μm < 1mm ≥2%
      富有机质纹层状灰质泥岩 Vsh≥50%,25≤Vca < 50%
      有机质纹层状云质泥岩 Vsh≥50%,25≤Vdo < 50%
      富有机质纹层状泥晶泥质灰岩 Vca≥50%,25≤Vsh < 50%
      富有机质纹层状微晶泥质灰岩 Vca≥50%,25≤Vsh < 50% ≥4 μm, < 30 μm
      富有机质纹层状微晶泥质云岩 Vdo≥50%,25≤Vsh < 50%
      富有机质纹层状粗晶泥质灰岩 Vca≥50%,25≤Vsh < 50% ≥30 μm
      富有机质层状灰质泥岩 Vsh≥50%,25≤Vca < 50% < 4 μm ≥1mm
      富有机质层状泥质灰岩 Vca≥50%,25≤Vsh < 50%
      富有机质块状泥岩 Vsh≥75% 纹层不发育
      含有机质纹层状粉砂质泥岩 Vsh≥50%,25≤Vsa < 50% < 1mm < 2%
      含有机质纹层状灰岩 Vca≥75% ≥4 μm, < 30 μm
      含有机质层状砂质泥岩 Vsh≥50%,25≤Vsa < 50% < 4 μm ≥1mm
      含有机质层状云质泥岩 Vsh≥50%,25≤Vdo < 50%
      含有机质层状膏质泥岩 Vsh≥50%,25≤Vgy < 50%
      含有机质层状砂质灰岩 Vca≥50%,25≤Vsa < 50%
      含有机质层状泥质云岩 Vdo≥50%,25≤Vsh < 50%
      含有机质块状泥岩 Vsh≥75% 纹层不发育
      含有机质块状灰岩 Vca≥75%
      含有机质块状云岩 Vdo≥75%
      注:Vsh.泥质含量;Vca.灰质含量;Vdo.云质含量;Vsa.砂质含量.
      下载: 导出CSV
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